湘中坳陷邵阳凹陷佘田桥组泥岩岩相及其成因演化

陈林; 张保民; 陈孝红; 蒋恕; 张国涛; 李海; 陈平; 林卫兵

doi:10.3799/dqkx.2020.253

Volume 46 Issue 4

Apr. 2021

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Article Navigation > Earth Science > 2021 > 46(4): 1282-1294

Chen Lin, Zhang Baomin, Chen Xiaohong, Jiang Shu, Zhang Guotao, Li Hai, Chen Ping, Lin Weibing, 2021. Lithofacies and Origin Evolution of Mudstone of Shetianqiao Formation in Shaoyang Sag of Xiangzhong Depression. Earth Science, 46(4): 1282-1294. doi: 10.3799/dqkx.2020.253

Citation:

Chen Lin, Zhang Baomin, Chen Xiaohong, Jiang Shu, Zhang Guotao, Li Hai, Chen Ping, Lin Weibing, 2021. Lithofacies and Origin Evolution of Mudstone of Shetianqiao Formation in Shaoyang Sag of Xiangzhong Depression. Earth Science, 46(4): 1282-1294. doi: 10.3799/dqkx.2020.253

Citation:

Chen Lin, Zhang Baomin, Chen Xiaohong, Jiang Shu, Zhang Guotao, Li Hai, Chen Ping, Lin Weibing, 2021. Lithofacies and Origin Evolution of Mudstone of Shetianqiao Formation in Shaoyang Sag of Xiangzhong Depression. Earth Science, 46(4): 1282-1294. doi: 10.3799/dqkx.2020.253

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Lithofacies and Origin Evolution of Mudstone of Shetianqiao Formation in Shaoyang Sag of Xiangzhong Depression

doi: 10.3799/dqkx.2020.253

Chen Lin^{1
,
,},
Zhang Baomin^{1
,
,
,},
Chen Xiaohong¹,
Jiang Shu^{2, 3},
Zhang Guotao¹,
Li Hai¹,
Chen Ping²,
Lin Weibing²

1.
Wuhan Center of China Geological Survey, Wuhan 430205, China
2.
Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Energy and Geoscience Institute, University of Utah, Salt Lake City 840108, United States

Received Date: 2020-05-29
Publish Date: 2021-04-15

Abstract

Abstract

The mudstone of the Devonian Shetianqiao Formation is one of the key strata for shale gas exploration in South China. In order to reveal the lithofacies characteristics and controlling factors of Shetianqiao Formation in Shaoyang sag of Xiangzhong depression, the lithofacies, sedimentary environment and its control on lithofacies development of mudstone were studied on the basis of systematical core description and test results of mineralogy and geochemistry, and the control of sedimentary environment evolution on lithofacies type is discussed in this study. Four lithofacies are identified, including siliceous mudstone, mixed mudstone, chert and calcareous mudstone, according to the differences of mineral component content. The Shetianqiao Formation can be divided into 5 lithofacies assemblages. Lithofacies assemblages Ⅰ and Ⅲ are relatively rich in silica, while the content of calcite in assemblages Ⅱ, Ⅳ, and Ⅴ is relatively high. The sedimentary environment analysis indicates that the mudstone of Shetianqiao Formation was formed at the continental margin setting. It was mainly developed in a relatively hot and dry climate, but the climate was relatively warm and humid in the early and middle stages. The middle stage developed the warmest and wettest climate. And the sea levels rose first and then fell in this period. The middle section is characterized by excess silica attributed to the biological origin and little influence by hydrothermal fluids. Terrestrial input was relatively stable and was the lowest in the middle stage. The coupling relationship between sedimentary environment and lithofacies types indicates that the lithofacies are mainly controlled by paleoclimate, terrestrial input, change in sea level, and biological origin. The siliceous components of mudstone are mainly contributed by the terrestrial input. The enriched silica in the middle section is mainly of biological origin. When the climate was hot and dry, the mudstone lithofacies was dominated by the calcium-riched lithofacies in the later period.
- Xiangzhong depression,
- Shaoyang sag,
- Shetianqiao Formation,
- mudstone,
- lithofacies,
- sedimentary environment,
- petrography

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References(65)

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Lithofacies and Origin Evolution of Mudstone of Shetianqiao Formation in Shaoyang Sag of Xiangzhong Depression

doi: 10.3799/dqkx.2020.253

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通讯作者: 陈斌, bchen63@163.com

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